UUnniivveerrssiittyy ooff SSoouutthh CCaarroolliinnaa SScchhoollaarr CCoommmmoonnss Theses and Dissertations 2017 MMoolleeccuullaarr EExxpplloorraattiioonn ooff BBiiooaavvaaiillaabbllee DDiissssoollvveedd OOrrggaanniicc MMaatttteerr AAccrroossss AAqquuaattiicc EEccoossyysstteemmss Yuan Shen University of South Carolina Follow this and additional works at: https://scholarcommons.sc.edu/etd Part of the Marine Biology Commons RReeccoommmmeennddeedd CCiittaattiioonn Shen, Y.(2017). Molecular Exploration of Bioavailable Dissolved Organic Matter Across Aquatic Ecosystems. (Doctoral dissertation). Retrieved from https://scholarcommons.sc.edu/etd/4231 This Open Access Dissertation is brought to you by Scholar Commons. It has been accepted for inclusion in Theses and Dissertations by an authorized administrator of Scholar Commons. For more information, please contact [email protected]. MOLECULAR EXPLORATION OF BIOAVAILABLE DISSOLVED ORGANIC MATTER ACROSS AQUATIC ECOSYSTEMS by Yuan Shen Bachelor of Science Xiamen University, 2009 Master of Science University of South Carolina, 2011 Submitted in Partial Fulfillment of the Requirements For the Degree of Doctor of Philosophy in Marine Science College of Arts and Sciences University of South Carolina 2017 Accepted by: Ronald Benner, Major Professor James Pinckney, Committee Member Lori Ziolkowski, Committee Member Karl Kaiser, Committee Member Cheryl L. Addy, Vice Provost and Dean of the Graduate School © Copyright by Yuan Shen, 2017 All Rights Reserved. ii DEDICATION I would like to dedicate this dissertation to my wife Jiani Zheng and my parents for all their love and support. iii ACKNOWLEDGEMENTS I would like to express my deepest appreciation to my advisor, Professor Ronald Benner, for his guidance, patience, encouragement, and support. His enthusiasm, vision, and creative thinking have been a great influence on me throughout my graduate studies. He made every project that we worked together so much enjoyable. One could not ask for a better advisor. I thank James Pinckney, Lori Ziolkowski, and Karl Kaiser for being on my committee and providing helpful comments and suggestions. I am very much thankful to Karl Kaiser and Cédric Fichot for teaching me the amino acid analysis and the DOC and CDOM analyses, respectively. I also thank my other lab mates and colleagues, Mike Philben, Oliver Lechtenfeld, Shengkang Liang, Qinghui Huang, Dandan Duan, Tae-Hoon Kim, Doug Bell, etc. for their companionship and the fun chatting on science and life. Special thanks go to my friends at the Gamecock Badminton Club (Richard Cheng, Xinyu Huang, Xinfeng Liu, Jo Evaristo, Xiaolong Liu, etc.), I appreciate their friendship and the good times that we spent together making my journey more joyful and memorable. Finally, I thank my collaborators for their contributions to this work and the US National Science Foundation for funding my research. iv ABSTRACT Dissolved organic matter (DOM) in aquatic ecosystems is a large reservoir of reduced carbon that is mostly resistant to degradation. A small fraction of DOM cycles relatively quickly and is biologically utilized on timescales of days to months. This bioavailable DOM (BDOM) supports aquatic food webs, drives major elemental cycles, and is coupled to atmospheric CO . Despite wide-ranging importance, bioavailability of 2 DOM and its linkages to ecosystem properties (e.g., primary production, nutrients) are poorly characterized, particularly at the ecosystem level. Bioassay experiments are commonly used to determine BDOM, but this approach alters conditions and has limited spatial and temporal coverage. In this dissertation, biochemical indicators of DOM bioavailability were developed and implemented in a wide range of ecosystems to reveal large-scale distributions of BDOM in the Arctic (Chapter 1) and Antarctic Oceans (Chapter 2), locate seasonal biological hotspots in a subtropical ocean margin (Chapter 3), and to trace transport and fate of BDOM from surface to ground waters (Chapter 4). Measurements of amino acids, a major bioactive component of BDOM, were compared between the high (Chukchi Sea) and low (Beaufort Sea) productivity regions of the western Arctic Ocean. Bulk concentrations of dissolved organic carbon (DOC) were similar in the two systems despite their contrasting productivity, but DOM bioavailability as indicated by amino acid yields was much higher in the more productive Chukchi Sea. Seasonal trends of amino acids revealed elevated production and rapid off-shelf transport of BDOM in the Chukchi Sea during a season with reduced sea-ice cover. v The use of amino acids as BDOM indicator was further tested in the Southern Ocean during austral winter when primary production is light-limited and minimal. The sampling encompassed ice-covered and ice-free waters along a latitudinal gradient in the region of the Antarctic Peninsula, one of the fastest warming regions on Earth. Unlike the DOC that varied irregularly, amino acid-based indices illustrated a significant northward increase in DOM bioavailability from ice-covered to open waters. Overall, the observations in the polar oceans indicate a correspondence between DOM bioavailability and nutrient- and light-driven changes in ecosystem productivity. A novel approach using two biochemical indicators (amino acids and carbohydrates) of BDOM was developed during a large-scale seasonal survey of the river-influenced Louisiana margin. These indicators revealed patchy distributions of compositionally distinct types of BDOM hotspots that varied with phytoplankton biomass and nutrient levels, and they further indicated a diel variability in sources of BDOM, with zooplankton grazing at night and phytoplankton extracellular release during daytime under nutrient limitation. Biochemical indicators were extended to surface and groundwater in South Carolina. Amino acids, lignin phenols, and chromophoric DOM were monitored monthly over two years. Linking groundwater DOM with surface water DOM and precipitation revealed differential transport of hydrophilic and hydrophobic molecules through soils and depletion of BDOM in groundwater. These observations guided a development of the Regional Chromatography Model to illustrate processes regulating the composition and bioavailability of DOM during transport through the soil column to the saturated zone. vi TABLE OF CONTENTS DEDICATION ....................................................................................................................... iii ACKNOWLEDGEMENTS ........................................................................................................ iv ABSTRACT ............................................................................................................................v LIST OF TABLES ................................................................................................................ viii LIST OF FIGURES ................................................................................................................. ix LIST OF ABBREVIATIONS ..................................................................................................... xi CHAPTER 1: DISSOLVED ORGANIC MATTER COMPOSITION AND BIOAVAILABILITY REFLECT ECOSYSTEM PRODUCTIVITY IN THE WESTERN ARCTIC OCEAN ............................................1 CHAPTER 2 BIOAVAILABLE DISSOLVED ORGANIC MATTER AND BIOLOGICAL HOT SPOTS DURING AUSTRAL WINTER IN ANTARCTIC WATERS ..........................................................29 CHAPTER 3 BIOLOGICAL HOT SPOTS AND THE ACCUMULATION OF MARINE DISSOLVED ORGANIC MATTER IN A HIGHLY PRODUCTIVE OCEAN MARGIN ........................................54 CHAPTER 4 ORIGINS AND BIOAVAILABILITY OF DISSOLVED ORGANIC MATTER IN GROUNDWATER ..................................................................................................................86 CHAPTER 5 OVERVIEW AND SYNTHESIS ...........................................................................120 REFERENCES .....................................................................................................................123 APPENDIX A – SUPPLEMENTARY TABLES .........................................................................143 APPENDIX B – SUPPLEMENTARY FIGURES ........................................................................144 APPENDIX C – PERMISSION TO REPRINT ...........................................................................146 vii LIST OF TABLES Table 1.1 Physicochemical characteristics in the Chukchi and Beaufort Seas .................19 Table 1.2 Comparisons of concentrations of DOC and TDAA, and TDAA yields ..........20 Table 1.3 Comparisons of concentrations of DOC and TDAA, and TDAA yields ..........21 Table 2.1 Summary of oceanographic parameters at the sampling stations ......................46 Table 2.2 Physicochemical properties of water masses and biological hotspots ..............47 Table 3.1 Average values and ranges for DOC, TDAA, and TDNS in the mixed layer during the five cruises on the Louisiana margin ................................................................75 Table 3.2 Concentrations and compositions of DOM during the shipboard bioassays .....76 Table 3.3 Surface mixed layer reservoirs of DOC on the Louisiana shelf .......................77 Table 4.1 DOC and amino acids in ground and surface waters and freshly-produced bacterial DOM .................................................................................................................106 Table 4.2 Optical properties of DOM in ground and surface waters ...............................108 Table 4.3 Correlation matrix between precipitation and DOM in groundwater ..............109 Table 4.4 Lignin phenols in ground and surface waters ..................................................110 Table 4.5 Yields of D-amino acids in freshly-produced bacterial DOM ........................111 viii LIST OF FIGURES Figure 1.1 Locations of sampling stations in the western Arctic Ocean ...........................22 Figure 1.2 Mixing patterns of DOM in the Mackenzie River plume ................................23 Figure 1.3 Concentrations of DOC in the Chukchi Sea and Beaufort Sea ........................24 Figure 1.4 Concentrations of TDAA in the Chukchi Sea and Beaufort Sea .....................25 Figure 1.5 DOC-normalized yields of TDAA in the Chukchi Sea and Beaufort Sea .......26 Figure 1.6 Average concentrations of DOC and TDAA, and TDAA yields in the Chukchi and Beaufort Seas ..............................................................................................................27 Figure 1.7 Average concentrations of DOC and TDAA, and TDAA yields in the Chukchi Sea between 2002 and 2004 ...............................................................................................28 Figure 2.1 Sampling sites off the South Shetland Islands (Antarctica) in August 2012 ...48 Figure 2.2 Distributions of temperature and salinity ........................................................49 Figure 2.3 Latitudinal distributions of chl-a and POC in different water masses .............50 Figure 2.4 Latitudinal distributions of DOC and TDAA in different water masses .........51 Figure 2.5 Profiles of chl-a, DOC, TDAA and POC at ice-free and ice-covered stations 52 Figure 2.6 Depth profiles of TDAA yields, glycine, nonprotein amino acids, and D-amino acids at four ice-free stations .............................................................................................53 Figure 3.1 Study area and sampling sites on the Louisiana margin ..................................78 Figure 3.2 Seasonal and spatial distributions of DOC, TDAA, and TDNS ......................79 Figure 3.3 Seasonal distributions of TDAA and TDNS yields .........................................80 Figure 3.4 Hot spots of labile DOM on the Louisiana margin ..........................................81 ix
Description: